Nuorten männiköiden kehitys - taimikonhoito ja ensiharvennus

The aim of this study was to investigate the effects of location, site type, regeneration method and precommercial thinning on the characteristics and development of young, even-aged, pure Scots pine stands. In addition, the effects of timing and intensity of first commercial thinning on the yield and profitability during the rotation period were also studied. The stand characteristics and external quality of young Scots pine stands and stand-level growth models were based on extensive inventory data of the Finnish Forest Research Institute for young Scots pine stands (3 measurement times, 192 stands). The effect of precommercial thinning on stand development was examined on the basis of long-term experiments (13 stands, 169 plots). The effect of timing and intensity of the first commercial thinning on yield and profitability were based on measurements made in first commercial thinnings (27 stands of Metsähallitus), and the further stand development was modeled using the MOTTI simulator. The thesis was based on four articles and a summary. Stand level growth models were developed for young, even-aged Scots pine stands. The models reliably predicted the development up until the first commercial thinning stage. The stand density of young Scots pine stands in Finland was moderately low compared to the target values. In addition, the external quality of pines was low on average. The low stand density and poor external quality will result in the need for quality tree selection in thinnings, if high quality sawn timber is required. In Northern Finland, only 20% of the dominant trees were classified as normal. This will lead to the situation where external quality will remain relatively poor up until the end of rotation. Early and light precommercial thinning (Hdom 3 m, to a density of 3000 trees per hectare) increased the thinning removal by 40% compared to late and more intensive precommercial thinning (at 7 meters to a density of 2000 trees per hectare). A model for the effect of precommercial thinning on merchantable thinning removal at the first commercial thinning was developed for forest management planning purposes. When the recommended time of first commercial thinning was delayed from a dominant height of 12 m to 16 m, or by ten years, the yield of merchantable wood was doubled. Simultaneously, the current value of the stumpage revenues (with 4% interest rate) was increased on the average by 65% (330 € per hectare). Variation in stumpage prices or interest rates did not have any effect on the final results. Without exception, delaying the first commercial thinning by ten years seemed to be the most profitable method. This presupposes that precommercial thinning has been carried out at the right time and that tree quality aspects do not be specially considered. Furthermore, the wood yield and economic outcome from the entire rotation were similar regardless of whether the first thinning was performed at the time currently recommended or ten years later.

Stand structural dynamics on pristine and managed boreal peatlands

The objectives of this study were to investigate the stand structure and succession dynamics in Scots pine (Pinus sylvestris L.) stands on pristine peatlands and in Scots pine and Norway spruce (Picea abies (L.) Karst.) dominated stands on drained peatlands. Furthermore, my focus was on characterising how the inherent and environmental factors and the intermediate thinnings modify the stand structure and succession. For pristine peatlands, the study was based on inventorial stand data, while for drained peatlands, longitudinal data from repeatedly measured stands were utilised. The studied sites covered the most common peatland site types in Finland. They were classified into two categories according to the ecohydrological properties related to microsite variation and nutrient levels within sites. Tree DBH and age distributions in relation to climate and site type were used to study the stand dynamics on pristine sites. On drained sites, the Weibull function was used to parameterise the DBH distributions and mixed linear models were constructed to characterise the impacts of different ecological factors on stand dynamics. On pristine peatlands, both climate and the ecohydrology of the site proved to be crucial factors determining the stand structure and its dynamics. Irrespective of the vegetation succession, enhanced site productivity and increased stand stocking they significantly affected the stand dynamics also on drained sites. On the most stocked sites on pristine peatlands the inter-tree competition seemed to also be a significant factor modifying stand dynamics. Tree age and size diversity increased with stand age, but levelled out in the long term. After drainage, the stand structural unevenness increased due to the regeneration and/or ingrowth of the trees. This increase was more pronounced on sparsely forested composite sites than on more fully stocked genuine forested sites in Scots pine stands, which further undergo the formation of birch and spruce undergrowth beneath the overstory as succession proceeds. At 20-30 years after drainage the structural heterogeneity started to decrease, indicating increased inter-tree competition, which increased the mortality of suppressed trees within stand. Peatland stands are more dynamic than anticipated and are generally not characterized by a balanced, self-perpetuating structure. On pristine sites, various successional pathways are possible, whereas on drained sites the succession has more uniform trend. Typically, stand succession proceeds without any distinct developmental stages on pristine peatlands, whereas on drained peatlands, at least three distinct stages could be identified. Thinnings had only little impact on the stand succession. The new information on stand dynamics may be utilised, e.g. in forest management planning to facilitate the allocation of the growth resources to the desired crop component by appropriate silvicultural treatments, as well as assist in assessing the effects of the climate change on the forested boreal peatlands.

Soil hydrological properties and conditions, site preparation, and the long-term performance of planted Scots pine (Pinus sylvestris L.) on upland forest sites in Finnish Lapland

Scots pine (Pinus sylvestris L.) and Norway spruce (Picea abies (L.) Karst.) forests dominate in Finnish Lapland. The need to study the effect of both soil factors and site preparation on the performance of planted Scots pine has increased due to the problems encountered in reforestation, especially on mesic and moist, formerly spruce-dominated sites. The present thesis examines soil hydrological properties and conditions, and effect of site preparation on them on 10 pine- and 10 spruce-dominated upland forest sites. Finally, the effects of both the site preparation and reforestation methods, and soil hydrology on the long-term performance of planted Scots pine are summarized. The results showed that pine and spruce sites differ significantly in their soil physical properties. Under field capacity or wetter soil moisture conditions, planted pines presumably suffer from excessive soil water and poor soil aeration on most of the originally spruce sites, but not on the pine sites. The results also suggested that site preparation affects the soil-water regime and thus prerequisites for forest growth over two decades after site preparation. High variation in the survival and mean height of planted pine was found. The study suggested that on spruce sites, pine survival is the lowest on sites that dry out slowly after rainfall events, and that height growth is the fastest on soils that reach favourable aeration conditions for root growth soon after saturation, and/or where the average air-filled porosity near field capacity is large enough for good root growth. Survival, but not mean height can be enhanced by employing intensive site preparation methods on spruce sites. On coarser-textured pine sites, site preparation methods don t affect survival, but methods affecting soil fertility, such as prescribed burning and ploughing, seem to enhance the height growth of planted Scots pines over several decades. The use of soil water content in situ as the sole criterion for sites suitable for pine reforestation was tested and found to be a relatively uncertain parameter. The thesis identified new potential soil variables, which should be tested using other data in the future.

Metsän kiertoajan vaikutus hiilensidontaan ja metsänkasvatuksen kannattavuuteen

Cost-effective mitigation of climate change is essential for both climate and environmental policy. Forest rotation age is one of the silvicultural measures by which the forest carbon stocks can be influenced with in accordance with the Kyoto Protocol, Article 3.4. The purpose of this study is to evaluate how forest rotation age affects carbon sequestration and the profitability of forestry. The relation between the forest rotation period optimizing forest owners’ discounted net returns over time and rotations which are 10, 20 and 30 years longer than the optimal rotation is examined. In addition, the cost of lengthening the rotation period is studied as well as whether carbon sequestration revenues can improve the profitability of forestry. The data used in the study consist of 16 stands located in Southern Finland. The main tree species in these stands were Norway spruce and Scots pine. Forest simulation tool MOTTI was used in the analysis. The results indicate that by lengthening the rotation period forest carbon stocks increase. However, as the rotation period is lengthened by more than 10 years, as a result of the diminishing growth curve, the rate of carbon sequestration slows down. The average discounted cost of carbon sequestration varied between 2.4 – 14.1 €/tCO2. Carbon sequestration rates in spruce stands were higher and the costs lower than those obtained from pine stands. The absence of carbon trading schemes is an obstacle for the commercialization of forest carbon sinks. In the future, research should concentrate on analysing what kind of operational models of carbon trading could be feasible in Finland.

Plant secondary compounds and soil microbial processes in carbon and nitrogen cycling in relation to tree species

The aim of this study was to explore soil microbial activities related to C and N cycling and the occurrence and concentrations of two important groups of plant secondary compounds, terpenes and phenolic compounds, under silver birch (Betula pendula Roth), Norway spruce (Picea abies (L.) Karst) and Scots pine (Pinus sylvestris L.) as well as to study the effects of volatile monoterpenes and tannins on soil microbial activities. The study site, located in Kivalo, northern Finland, included ca. 70-year-old adjacent stands dominated by silver birch, Norway spruce and Scots pine. Originally the soil was very probably similar in all three stands. All forest floor layers (litter (L), fermentation layer (F) and humified layer (H)) under birch and spruce showed higher rates of CO2 production, greater net mineralisation of nitrogen and higher amounts of carbon and nitrogen in microbial biomass than did the forest floor layers under pine. Concentrations of mono-, sesqui-, di- and triterpenes were higher under both conifers than under birch, while the concentration of total water-soluble phenolic compounds as well as the concentration of condensed tannins tended to be higher or at least as high under spruce as under birch or pine. In general, differences between tree species in soil microbial activities and in concentrations of secondary compounds were smaller in the H layer than in the upper layers. The rate of CO2 production and the amount of carbon in the microbial biomass correlated highly positively with the concentration of total water-soluble phenolic compounds and positively with the concentration of condensed tannins. Exposure of soil to volatile monoterpenes and tannins extracted and fractionated from spruce and pine needles affected carbon and nitrogen transformations in soil, but the effects were dependent on the compound and its molecular structure. Monoterpenes decreased net mineralisation of nitrogen and probably had a toxic effect on part of the microbial population in soil, while another part of the microbes seemed to be able to use monoterpenes as a carbon source. With tannins, low-molecular-weight compounds (also compounds other than tannins) increased soil CO2 production and nitrogen immobilisation by soil microbes while the higher-molecular-weight condensed tannins had inhibitory effects. In conclusion, plant secondary compounds may have a great potential in regulation of C and N transformations in forest soils, but the real magnitude of their significance in soil processes is impossible to estimate.

Postglacial climate changes and vegetation responses in northern Europe

Postglacial climate changes and vegetation responses were studied using a combination of biological and physical indicators preserved in lake sediments. Low-frequency trends, high-frequency events and rapid shifts in temperature and moisture balance were probed using pollen-based quantitative temperature reconstructions and oxygen-isotopes from authigenic carbonate and aquatic cellulose, respectively. Pollen and plant macrofossils were employed to shed light on the presence and response rates of plant populations in response to climate changes, particularly focusing on common boreal and temperate tree species. Additional geochemical and isotopic tracers facilitated the interpretation of pollen- and oxygen-isotope data. The results show that the common boreal trees were present in the Baltic region (~55°N) during the Lateglacial, which contrasts with the traditional view of species refuge locations in the south-European peninsulas during the glacial/interglacial cycles. The findings of this work are in agreement with recent paleoecological and genetic evidence suggesting that scattered populations of tree species persisted at higher latitudes, and that these taxa were likely limited to boreal trees. Moreover, the results demonstrate that stepwise changes in plant communities took place in concert with major climate fluctuations of the glacial/interglacial transition. Postglacial climate trends in northern Europe were characterized by rise, maxima and fall in temperatures and related changes in moisture balance. Following the deglaciation of the Northern Hemisphere and the early Holocene reorganization of the ice-ocean-atmosphere system, the long-term temperature trends followed gradually decreasing summer insolation. The early Holocene (~11,700-8000 cal yr BP) was overall cool, moist and oceanic, although the earliest Holocene effective humidity may have been low particularly in the eastern part of northern Europe. The gradual warming trend was interrupted by a cold event ~8200 cal yr BP. The maximum temperatures, ~1.5-3.0°C above modern values, were attained ~8000-4000 cal yr BP. This mid-Holocene peak warmth was coupled with low lake levels, low effective humidity and summertime drought. The late Holocene (~4000 cal yr BP-present) was characterized by gradually decreasing temperatures, higher lake levels and higher effective humidity. Moreover, the gradual trends of the late Holocene were probably superimposed by higher-frequency variability. The spatial variability of the Holocene temperature and moisture balance patterns were tentatively attributed to the differing heat capacities of continents and oceans, changes in atmospheric circulation modes and position of sites and subregions with respect to large water bodies and topographic barriers. The combination of physical and biological proxy archives is a pivotal aspect of this work, because non-climatic factors, such as postglacial migration, disturbances and competitive interactions, can influence reshuffling of vegetation and hence, pollen-based climate reconstructions. The oxygen-isotope records and other physical proxies presented in this work manifest that postglacial climate changes were the main driver of the establishment and expansion of temperate and boreal tree populations, and hence, large-scale and long-term vegetation patterns were in dynamic equilibrium with climate. A notable exception to this pattern may be the postglacial invasion of Norway spruce and the related suppression of mid-Holocene temperate forest. This salient step in north-European vegetation history, the development of the modern boreal ecosystem, cannot be unambiguously explained by current evidence of postglacial climate changes. The results of this work highlight that plant populations, including long-lived trees, may be able to respond strikingly rapidly to changes in climate. Moreover, interannual and seasonal variation and extreme events can exert an important influence on vegetation reshuffling. Importantly, the studies imply that the presence of diffuse refuge populations or local stands among the prevailing vegetation may have provided the means for extraordinarily rapid vegetation responses. Hence, if scattered populations are not provided and tree populations are to migrate long distances, their capacity to keep up with predicted rates of future climate change may be lower than previously thought.

Nuorten mäntyjen ulkoisen laadun kehitykseen vaikuttavat tekijät

Männyn laatuun vaikuttavista tekijöistä tässä tutkimuksessa selvitettiin, mitkä tekijät aiheuttavat nuorissa männyissä oksikkuutta, mutkaisuutta käsittäen myös lenkouden ja haaraisuutta. Jokaiselle laatuvialle laadittiin kolme eritasoista mallia. Eniten keskityttiin tutkimaan oksikkuutta aiheuttavia tekijöitä, koska oksikkuus vaikuttaa männyn sisäiseen oksaisuuteen, joka on yleisin sahatavarakappaleen laatuluokan määräävä ominaisuus. Lisäksi mutkaisuus ja erityisesti haaraisuus osoittautuivat melko sattumanvaraisesti esiintyviksi laatuvioiksi, minkä takia niiden kehittymiseen vaikuttavia tekijöitä on vaikea määritellä. Tutkimuksessa käytettiin Metsäntutkimuslaitoksen taimikoiden inventointikokeiden (TINKA-kokeet) aineiston ensimmäisen ja kolmannen mittauskerran tuloksia. Näiden mittauskertojen väli oli 15 vuotta. Tutkimuksen perustuminen useampaan kuin yhteen mittauskertaan erottaa tämän tutkimuksen monista muista mäntyjen laatua käsittelevistä tutkimuksista, jotka ovat perustuneet yhden mittauskerran poikkileikkausaineistoon. Laadittujen kolmen eritasoisen mallin perusteella voidaan todeta, että oksikkuuden ja mutkaisuuden kehittymistä mäntyihin pystytään arvioimaan kohtalaisesti jo metsikön perustietojen (syntytapa, kasvupaikka, lämpösumma) avulla, jotka metsänomistajalla on tiedossaan jo taimikkoa perustaessaan. Puutason mittauksilla pystytään selvästi tarkentamaan arviota siitä, tuleeko männystä oksikas vai ei. Sitä vastoin puutason mittaukset parantavat vain vähän arviota mutkaisuuden kehittymisestä. Haaraisuuden esiintymistä luotettavasti ennustavaa mallia ei pystytty tekemään. Oksikkuutta lisääviä tekijöitä mallien mukaan olivat mm. männyn suuri läpimitan kasvu, suuri suhteellinen pituus saman metsikön muihin puihin verrattuna, alhainen kasvatustiheys männyntaimikon alkukehitysvaiheessa ja taimikonhoidon tekemättä jättäminen. Mutkaisuutta lisääviä tekijöitä olivat mm. suuri lämpösumma eli männikön sijainti Etelä-Suomessa, männyn suuri läpimitan kasvu, pieni suhteellinen pituus, alhainen kasvatustiheys männyntaimikon alkukehitysvaiheessa ja taimikonhoidon tekemättä jättäminen. Eri uudistamistavoista kylvö osoittautui parhaimmaksi laadun kannalta sekä oksikkuutta että mutkaisuutta tarkasteltaessa. Haaraisuutta lisääviä tekijöitä olivat mm. pieni lämpösumma eli männikön sijainti Pohjois-Suomessa, männyn suuri läpimitan kasvu ja alhainen kasvatustiheys männyntaimikon alkukehitysvaiheessa.

Männyn neulaskadon arviointi laserkeilauksella

Leaf and needle biomasses are key factors in forest health. Insects that feed on needles cause growth losses and tree mortality. Insect outbreaks in Finnish forests have increased rapidly during the last decade and due to climate change the damages are expected to become more serious. There is a need for cost-efficient methods for inventorying these outbreaks. Remote sensing is a promising means for estimating forests and damages. The purpose of this study is to investigate the usability of airborne laser scanning in estimating Scots pine defoliation caused by the common pine sawfly (Diprion pini L.). The study area is situated in Ilomantsi district, eastern Finland. Study materials included high-pulse airborne laser scannings from July and October 2008. Reference data consisted of 90 circular field plots measured in May-June 2009. Defoliation percentage on these field plots was estimated visually. The study was made on plot-level and methods used were linear regression, unsupervised classification, Maximum likelihood method, and stepwise linear regression. Field plots were divided in defoliation classes in two different ways: When divided in two classes the defoliation percentages used were 0–20 % and 20–100 % and when divided in four classes 0–10 %, 10–20 %, 20–30 % and 30–100 %. The results varied depending on method and laser scanning. In the first laser scanning the best results were obtained with stepwise linear regression. The kappa value was 0,47 when using two classes and 0,37 when divided in four classes. In the second laser scanning the best results were obtained with Maximum likelihood. The kappa values were 0,42 and 0,37, correspondingly. The feature that explained defoliation best was vegetation index (pulses reflected from height > 2m / all pulses). There was no significant difference in the results between the two laser scannings so the seasonal change in defoliation could not be detected in this study.

Metsikön rakenteen vaikutus säteilyn sammumiskertoimeen

Kasvuston G-funktio kuvaa säteilyn vähenemistä tai ”sammumista” auringon eri korkeuskulmissa varjostavan lehtialan suhteen. Sen vuoksi sitä kutsutaan sammumiskertoimeksi. Tutkimuksen tavoitteena oli selvittää vaihteleeko G-funktion muoto eri puulajien metsiköissä, ja voidaanko puulajit erottaa toisistaan G-funktion muodon avulla. Arvioin lisäksi G-funktioiden muodossa kasvukaudenaikana tapahtuvia muutoksia. Muita tutkimuksen kannalta mielenkiintoisia tutkimuskysymyksiä olivat voidaanko ryhmittymistä tai latvusmuotoa arvioida G-funktion muodon avulla. Maastomittaukset suoritettiin 3.5.2010 -30.9.2010 välisenä aikana. Tutkimusalueena oli Hyytiälän metsäaseman (68?59`N, 35?72`E) ympäristö, jonka metsät edustavat tyypillistä boreaalista havu- ja lehtimetsää. Tutkimusta varten perustettiin kuusi yhden puulajin koealaa, kaksi kutakin puulajia kohden. Tutkittavat puulajit olivat mänty (Pinus sylvestris), kuusi (Picea abies) ja rauduskoivu (Betula pendula). Koealaparit valittiin niin, että kullekin puulajille muodostui varttuneesta metsästä ja taimikosta muodostuva pari tai vaihtoehtoisesti tiheämpi ja harvempi koeala. Koealoille perustettiin 81 mittauspistettä sisältävä mittaushila, jossa kunkin pisteen aukkoisuustiedot mitattiin kahden viikon välein. Mittaukset suoritettiin kahdella LAI-2000 Plant Canopy Analyzer -laitteella. Laitteiden tulosteista koealoille saatiin aukkoisuustiedot T(?) ja LAI, joiden avulla saatiin laskettua tarkasteltavat G-funktiot. Saman puulajin G-funktiota vertailtiin toisiinsa puulajityypillisten trendien havaitsemiseksi. Keskikesällä eri puulajien G-funktioita verrattiin toisiinsa. Teoreettisten simulointien avulla tutkittiin latvuksen dimensioiden (latvuksen pituus ja säde) ja sisäisen ryhmittäisyyden vaikutusta puulajikohtaiseen G-funktioon. Simuloinneissa käytettiin hyväksi tietoa koealojen puustotunnuksista, lehtialasta sekä runkoluvusta. Puulajikohtaiset G-funktiot ovat erotettavissa toisistaan funktion minimi- ja maksimiarvojen sijoittumisen sekä suhteellisen vaihteluvälin perusteella. Havupuualojen G-funktiot eivät juuri muuttuneet kasvukauden aikana. Koivualoilla G-funktion kasvukaudenaikaiset muutokset (pelkät oksat, hiirenkorvat ja täysikasvuiset lehdet) olivat sitä vastoin helposti havaittavissa. G-funktion muodon avulla voidaan myös arvioida latvusmuotoa ja ryhmittymistä. Mäntyjen latvusmuoto on approksimoitavissa parhaiten ympyräkartion avulla. Kuusien ja koivujen latvusmuodon approksimointiin parhaana vaihtoehtona voidaan pitää ellipsoidia. Teoreettisten simulointien perusteella nuori kuusikko on muita havupuualoja ryhmittyneempi. Tutkimuksen mukaan säteily sammuu satelliittien yleisimmässä kuvaussuunnassa tehokkaammin kuin kaikkien suuntien yli laskettu keskiarvo (0,5) antaa olettaa. Puulajikohtaisten G-funktioiden avulla voidaan epäsuorasti arvioida sekä metsästä tapahtuvaa heijastusta että metsikön sisäisiä säteilyolosuhteita, sillä puulaji yhdessä metsikön rakenteen kanssa vaikuttaa metsästä heijastuvaan säteilyyn. Puulajikohtainen G-funktio on parametri, jonka avulla voidaan kalibroida malleja, joissa tarvitaan tietoa säteilyn kulusta erilaisissa kasvustoissa.

Turvemaan männyn (Pinus sylvestris L.) ja kuusen (Picea abies [L.] Karst.) kanto- ja juuripuun ominaisuudet ja asetoniliukoisten uuteaineiden määrä

Tutkimus on osa Metsäklusteri Oy:n Future Biorefinery –tutkimusohjelmaa, jossa kartoitetaan mahdollisuuksia hyödyntää metsäteollisuuden raaka-aineita aiempaa tarkemmin ja uusissa tuotteissa. Tutkimuksen tavoitteena on selvittää männyn (Pinus sylvestris L.) ja kuusen (Picea abies [L.] Karst.) juurten ja kantopuun rakenne ja ominaisuudet. Tutkimuksessa selvitetään löytyykö männyn ja kuusen juurista reaktiopuuta ja määritetään asetoniliukoisten uuteaineiden osuus kantoja juuripuussa. Tutkimusaineistona oli viisi eri-ikäistä mäntyä ja viisi eri-ikäistä kuusta. Juuri- ja kantoaineisto kerättiin Metsäntutkimuslaitoksen toimesta Parkanon seudulta (62.017°N, 23.017°E) hakkuun jälkeen. Maanalaisista juurista otettiin näytteet kolmelta eri etäisyydeltä juurenniskaan nähden. Kummankaan lajin juurista ei löytynyt varsinaista reaktiopuuta, mutta joissakin näytteissä havaittiin lievää reaktiopuuta. Lievää reaktiopuuta löytyi enemmän männyn kuin kuusen juurista, eikä sitä löytynyt lainkaan kaikkein ohuimmista, noin 2 cm paksuisista juurenosista. Männyn kannoissa uuteaineprosentti oli korkeampi kuin kuusen. Männyn juurissa uuteaineprosentti kasvoi edettäessä kohti juuren kärkeä. Kuusella uuteaineprosentti laski aluksi, mutta lähellä juuren kärkeä taas kasvoi. Kuoren uuteainepitoisuus oli molemmilla puulajeilla korkeampi kuin puuaineen. Tutkimusaineisto oli suppea, eikä tutkimuksessa pyritty tilastolliseen yleistettävyyteen. Laajemmasta aineistosta tehdylle tutkimukselle on tarvetta, sillä turvekankailta saatavan puun tarjonta on Suomessa kasvussa, mutta juurten uuteaine- ja reaktiopuututkimuksia on tehty vain kivennäismailta kerätyistä aineistoista.

Metsämaan vesitaseen muutokset Suomessa ilmaston muuttuessa

Muuttuva ilmasto, erityisesti kohoava lämpötila ja hiilidioksidipitoisuus, ei voi olla vaikuttamatta metsien kasvuun Suomessa. Metsätalouden sopeutumistoimilla voidaan pyrkiä lisääntyvän tuotospotentiaalin hyödyntämiseen ja metsätuhoriskien pienentämiseen. Sopeutumistoimien suunnittelemiseksi tarvitaan kuitenkin ensin tietoa siitä, miten ilmasto muuttuu ja mitä vaikutuksia ilmastonmuutoksella on. Työni oli osa vuonna 2005 käynnistettyä Ilmastonmuutoksen sopeutumistutkimusohjelmaa (ISTO). ISTO, ja näin myös oma tutkimukseni, tuottaa siis tietoa, jonka avulla voidaan mukauttaa metsänhoitoa vastaamaan muuttuvia ilmastooloja. Työssä tarkasteltiin maan vesipitoisuutta menneessä, nykyisessä ja muuttuvassa ilmastossa. Tavoitteena oli ennustaa, miten kuivuuden esiintyminen muuttuu Suomessa. Lisäksi menneiden kuivien vuosien kasvuvaikutuksia tutkittiin lustomittausten avulla. Vesitasemuutoksia lähdettiin tutkimaan mallilaskelmilla. Laskelmat perustuivat yksinkertaiseen open bucket – tyyppiseen vesimalliin. Mallissa maaperä ajatellaan tilana, johon sadanta ja lumen sulaminen tuovat vettä. Haihdunta ja valunta päinvastaisesti vähentävät sitä. Mallia sovellettiin Metlan yhdeksällä provenienssikoealueella, joihin lukeutui sekä kuusikoita että männiköitä eri kasvupaikoilta. Mallin yksinkertaisuuden takia koealueilta tarvittiin ainaostaan päivittäiset tiedot lämpötilasta, sadannasta, säteilystä ja VPD:stä. Lisäksi tuli selvittää kasvupaikkojen savi- ja hiekkapitoisuudet maaperäparametrien laskemiseksi. Vesimallilla tehtiin kahdet laskelmat. Ensimmäisissä laskettiin päivittäistä vesitasetta vuosina 1961-2008 mitattua sääaineistoa käyttäen. Toisissa laskelmissa käytettiin mitatusta säädatasta modifioitua sääennustetta. Lämpötilaa ja sadantaa oli kasvatettu vastaamaan vuosisadan lopulle tehtyä ennustetta. Näiden kahden laskelman tuloksia vertailtiin keskenään kuivuuspäivien lukumäärän osalta. Malliin oli siis ohjelmoitu kuivuuspäiväindeksi. Indeksin perusteella kuivuutta katsottiin olleen päivänä, jolloin kasveille käyttökelpoisen veden määrä laski alle 4 prosentin ja haihdunta leikkaantui 90 prosentilla normaalitasoon nähden. Kuivuuspäivät lisääntyivät kaikilla provenienssikoealueilla. Suurin muutos olisi tulosten perusteella odotettavissa etelärannikolla ja männyn kasvupaikoilla, jotka jo entuudestaan olivat alueista kuivimpia. Vähäisin muutos olisi taas odotettavissa kuusen kasvupaikoilla, etenkin jos sijainti ei ole aivan eteläisimmässä Suomessa. Kasvuvaikutuksia koskevien tulosten perusteella maan vesipitoisuus ei ole ollut merkittävä lustojen kasvua rajoittava tekijä provenienssikoealueilla menneinä vuosikymmeninä. Kuivuuspäivien määriin ei tule suhtautua absoluuttisina totuuksina, sillä ne ovat määritelmänsä mukaisesti vain suuntaa antavia. Niiden avulla voidaan tehdä ainoastaan päätelmiä metsiköiden ja vuosien välisistä suhteellisista eroista ja kehityssuunnista. Suoria johtopäätöksiä puuston kasvusta tai elinvoimaisuudesta ei pystytä tekemään. Eikä myöskään pystytä arvioimaan, reagoivatko mänty ja kuusi ennustettuihin muutoksiin eri tavoin. Voidaan kuitenkin päätellä, että keskimääräisten vuotuisten kuivuuspäivien lukumäärän kasvu johtaa brutto- ja nettoprimäärituotoksen vähenemiseen. Tätä kautta kuivuuden lisääntyminen alentaa myös kasvua verrattuna tilanteeseen, jossa kuivuuspäivien määrä pysyisi muuttumattomana.

Understorey vegetation as an indicator of forest site potential in Southern Finland.

The relationship between site characteristics and understorey vegetation composition was analysed with quantitative methods, especially from the viewpoint of site quality estimation. Theoretical models were applied to an empirical data set collected from the upland forests of southern Finland comprising 104 sites dominated by Scots pine (Pinus sylvestris L.), and 165 sites dominated by Norway spruce (Picea abies (L.) Karsten). Site index H100 was used as an independent measure of site quality. A new model for the estimation of site quality at sites with a known understorey vegetation composition was introduced. It is based on the application of Bayes' theorem to the density function of site quality within the study area combined with the species-specific presence-absence response curves. The resulting posterior probability density function may be used for calculating an estimate for the site variable. Using this method, a jackknife estimate of site index H100 was calculated separately for pine- and spruce-dominated sites. The results indicated that the cross-validation root mean squared error (RMSEcv) of the estimates improved from 2.98 m down to 2.34 m relative to the "null" model (standard deviation of the sample distribution) in pine-dominated forests. In spruce-dominated forests RMSEcv decreased from 3.94 m down to 3.16 m. In order to assess these results, four other estimation methods based on understorey vegetation composition were applied to the same data set. The results showed that none of the methods was clearly superior to the others. In pine-dominated forests, RMSEcv varied between 2.34 and 2.47 m, and the corresponding range for spruce-dominated forests was from 3.13 to 3.57 m.

Heating values of mature trees.

The effective heating values of the above and below ground biomass components of mature Scots pine (Pinus sylvestris), Norway spruce (Picea abies), downy birch (Betula pubescens), silver birch (Betula pendula), grey alder (Alnus incana), black alder (Alnus glutinosa) and trembling aspen (Populus tremula) were studied. Each sample tree was divided into wood, bark and foliage components. Bomb calorimetry was used to determine the calorimetric heating values. The species is a significant factor in the heating value of individual tree components. The heating value of the wood proper is highest in conifers. Broad-leaved species have a higher heating value of bark than conifers. The species factor diminishes when the weighted heating value of crown, whole stems or stump-root-system are considered. The crown material has a higher heating value per unit weight in comparison with fuelwood from small-sized stems or wholetrees. The additional advantages of coniferous crown material are that it is a non-industrial biomass resource and is readily available. The variability of both the chemical composition and the heating value is small in any given tree component of any species. However, lignin, carbohydrate and extractive content were found to vary from one part of the tree to another and to correlate with the heating value.

Pre-harvest measurement of pine stands for sawing production planning.

To enhance the utilization of the wood, the sawmills are forced to place more emphasis on planning to master the whole production chain from the forest to the end product. One significant obstacle to integrating the forest-sawmill-market production chain is the lack of appropriate information about forest stands. Since the wood procurement point of view in forest planning systems has been almost totally disregarded there has been a great need to develop an easy and efficient pre-harvest measurement method, allowing separate measurement of stands prior to harvesting. The main purpose of this study was to develop a measurement method for pine stands which forest managers could use in describing the properties of the standing trees for sawing production planning. Study materials were collected from ten Scots pine stands (Pinus sylvestris) located in North Häme and South Pohjanmaa, in southern Finland. The data comprise test sawing data on 314 pine stems, dbh and height measures of all trees and measures of the quality parameters of pine sawlog stems in all ten study stands as well as the locations of all trees in six stands. The study was divided into four sub-studies which deal with pine quality prediction, construction of diameter and dead branch height distributions, sampling designs and applying height and crown height models. The final proposal for the pre-harvest measurement method is a synthesis of the individual sub-studies. Quality analysis resulted in choosing dbh, distance from stump height to the first dead branch (dead branch height), crown height and tree height as the most appropriate quality characteristics of Scots pine. Dbh and dead branch height are measured from each pine sample tree while height and crown height are derived from dbh measures by aid of mixed height and crown height models. Pine and spruce diameter distribution as well as dead branch height distribution are most effectively predicted by the kernel function. Roughly 25 sample trees seems to be appropriate in pure pine stands. In mixed stands the number of sample trees needs to be increased in proportion to the intensity of pines in order to attain the same level of accuracy.

Production process of Scots pine.

The accompanying collective research report is the result of the research project in 1986­90 between The Finnish Academy and the former Soviet Academy of Sciences. The project was organized around common field work in Finland and in the former Soviet Union and theoretical analyses of tree growth determining processes. Based on theoretical analyses, dynamic stand growth models were made and their parameters were determined utilizing the field results. Annual cycle affects the tree growth. Our theoretical approach was based on adaptation to local climate conditions from Lapland to South Russia. The initiation of growth was described as a simple low and high temperature accumulation driven model. Linking the theoretical model with long term temperature data allowed us to analyze what type of temperature response produced favorable outcome in different climates. Initiation of growth consumes the carbohydrate reserves in plants. We measured the dynamics of insoluble and soluble sugars in the very northern and Karelian conditions. Clear cyclical pattern was observed but the differences between locations were surprisingly small. Analysis of field measurements of CO2 exchange showed that irradiance is the dominating factor causing variation in photosynthetic rate in natural conditions during summer. The effect of other factors is so small that they can be omitted without any considerable loss of accuracy. A special experiment carried out in Hyytiälä showed that the needle living space, defined as the ratio between the shoot cylindric volume and needle surface area, correlates with the shoot photosynthesis. The penetration of irradiance into Scots pine canopy is a complicated phenomenon because of the movement of the sun on the sky and the complicated structure of branches and needles. A moderately simple but balanced forest radiation regime submodel was constructed. It consists of the tree crown and forest structure, the gap probability calculation and the consideration of spatial and temporal variation of radiation inside the forest. The common field excursions in different geographical regions resulted in a lot of experimental data of regularities of woody structures. The water transport seems to be a good common factor to analyse these properties of tree structure. There are evident regressions between cross-sectional areas measured at different locations along the water pathway from fine roots to needles. The observed regressions have clear geographical trends. For example, the same cross-sectional area can support three times higher needle mass in South Russia than in Lapland. Geographical trends can also be seen in shoot and needle structure. Analysis of data published by several Russian authors show, that one ton of needles transpire 42 ton of water a year. This annual amount of transpiration seems to be independent of geographical location, year and site conditions. The produced theoretical and experimental material is utilised in the development of stand growth model that describes the growth and development of Scots pine stands in Finland and the former Soviet Union. The core of the model is carbon and nutrient balances. This means that carbon obtained in photosynthesis is consumed for growth and maintenance and nutrients are taken according to the metabolic needs. The annual photosynthetic production by trees in the stand is determined as a function of irradiance and shading during the active period. The utilisation of the annual photosynthetic production to the growth of different components of trees is based on structural regularities. Since the fundamental metabolic processes are the same in all locations the same growth model structure can be applied in the large range of Scots pine. The annual photosynthetic production and structural regularities determining the allocation of resources have geographical features. The common field measurements enable the application of the model to the analysis of growth and development of stands growing on the five locations of experiments. The model enables the analysis of geographical differences in the growth of Scots pine. For example, the annual photosynthetic production of a 100-year-old stand at Voronez is 3.5 times higher than in Lapland. The share consumed to needle growth (30 %) and to growth of branches (5 %) seems to be the same in all locations. In contrast, the share of fine roots is decreasing when moving from north to south. It is 20 % in Lapland, 15 % in Hyytiälä Central Finland and Kentjärvi Karelia and 15 % in Voronez South Russia. The stem masses (115­113 ton/ha) are rather similar in Hyytiälä, Kentjärvi and Voronez, but rather low (50 ton/ha) in Lapland. In Voronez the height of the trees reach 29 m being in Hyytiälä and Kentjärvi 22 m and in Lapland only 14 m. The present approach enables utilization of structural and functional knowledge, gained in places of intensive research, in the analysis of growth and development of any stand. This opens new possibilities for growth research and also for applications in forestry practice.